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    P E R U

    PROEXPLO 2005

    May 24-27, Lima

    BUILDING MINES, DELIVERING VALUE

    SOUTH AMERICA OVERVIEW

    &

    THE LAGUNAS NORTE GOLD DEPOSIT,ALTO CHICAMA DISTRICT, NORTHERN PERU

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    P E R U

    PROEXPLO 2005

    May 24-27, Lima

    FORWARD LOOKING STATEMENT

    Certain statements included herein, including those regarding production, costs, development schedules

    and other statements that express managements expectations or estimates of our future performance,

    constitute forward-looking statements within the meaning of the United States Private SecuritiesLitigation Reform Act of 1995. The words believe, expect, anticipate, contemplate, target,

    plan, intends, continue, budget, estimate, may, will, schedule, and similar expressions

    identify forward-looking statements. Forward-looking statements are necessarily based upon a number of

    estimates and assumptions that, while considered reasonable by management are inherently subject to

    significant business, economic and competitive uncertainties and contingencies. We caution you that such

    forward-looking statements involve known and unknown risks, uncertainties and other factors that may

    cause the actual financial results, performance or achievements of Barrick to be materially different from

    our estimated future results, performance or achievements expressed or implied by those forward-looking

    statements and our forward-looking statements are not guarantees of future performance. These risks,

    uncertainties and other factors include, but are not limited to: changes in the worldwide price of gold or

    certain other commodities (such as silver, copper, diesel fuel and electricity) and currencies; changes in

    interest rates or gold lease rates that could impact realized prices under our forward sales program;

    legislative, political or economic developments in the jurisdictions in which Barrick carries on business;

    operating or technical difficulties in connection with mining or development activities; the speculative

    nature of gold exploration and development, including the risks of diminishing quantities or grades of

    reserves; and the risks involved in the exploration, development and mining business. These factors arediscussed in greater detail in Barricks most recent Form 40-F/Annual Information on file with the U.S.

    Securities and Exchange Commission and Canadian provincial securities regulatory authorities.

    Barrick expressly disclaims any intention or obligation to update or revise any forward-looking statements

    whether as a result of new information, events or otherwise.

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    PROEXPLO 2005

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    PROEXPLO 2005

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    PROEXPLO 2005

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    PROEXPLO 2005

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    SUMMMMARY GOLD MINERAL RESERVES

    & RESOURCES, 2004

    ABX Barrick SA

    Gold 110 Moz 46 Moz

    Silver 911 Moz 879 Moz

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    P E R U

    PROEXPLO 2005

    May 24-27, Lima

    Pascua-Lama

    El Indio-Tambo

    Veladero

    Alto Chicama

    Pierina

    BARRI CKS MI NES & PROJECTS GOLD MI NERAL RESERVES

    9.1 mil lion ounces

    2.5 mil lion ounces

    (after 5 Moz depleted)

    17.6 million ounces

    12.8 million ounces

    (5.3 Moz depleted)

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    PROEXPLO 2005

    May 24-27, Lima

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    Orebody occurs as 750m x 3000m t abular blanket t rending ~ 345,betw een ~ 4050 and 4350m elevat ion

    Disseminated Au+ Ag mineralization associated w it h shallow-levelhigh-sulf idat ion alt erat ion similar t o Pierina, Alt o Chicama, Pascua

    Ore is characterized by mult iple stages of brecciat ion, alt erat ion, andprecious metal m ineralization

    Maj or cont rols on mineralization are fracture

    int ensit y, porosit y, st ructural intersect ions,silicificat ion, and elevat ion

    Veladero GeologyVeladero Geology

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    P E R U

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    May 24-27, Lima

    Veladero ProjectVeladero Project

    Locat ed in San Juan Province, Argent ina; 6kilomet ers f rom t he Pascua-Lama proj ect in t heFront era Dist r ict

    Open-pit , valley-f i l l heap leach operat ion w it htw o-st age crushing, sim ilar t o Barr ick s Pierina

    Mine

    Merger w it h Homestake Mining Company inDecember 2001 gave Barr ick 100% of Veladero;

    formerly a j oint venture ow ned 40% and 60% by

    Barr ick and Homest ake, respect ively

    Proven and probable gold reserves of 12.8 mil lion

    ounces

    Veladero ProjectVeladero Project

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    P E R U

    PROEXPLO 2005

    May 24-27, Lima

    Act ivi t ies Underw ay

    Const ruct ion at t he proj ect is about 80% complete as at Q1,2005

    Placement of t he valley-f ill heap leach secondary liner is

    complete and the primary l iner is 75% complete

    Stacking of ore commenced in Q1, 2005Process plant st eel erect ion in about 85% complete

    Product ion t argeted to comm ence in Q4, 2005

    Dril l ing around t he mine sit e began in late 2004 w it h posit ive

    result s at Guanaco Zonzo (approx. 5km from Veladero)

    Const ruct ion Cost Est imat e Approximately $540mil l ion

    Gold product ion is expected t o averageapproximat ely 700,000 ounces per year

    at an average total cash cost of

    about $200 per ounce(over t he first full t hree years)

    Veladero ProjectVeladero Project

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    Part of t he 30-m ill ion-ounce Front era Dist rict st raddling t heborder of Chile and Argent ina

    Barr ick plans t o develop Pascua-Lama as part of a uni f ieddist rict, st art ing w it h Veladero in 2005

    Proven and probable gold reserves of 17.6 m ill ion ounces;

    Silver contained w it hin report edgold reserves of 643 million ounces

    Pascua-Lama Proj ectPascua-Lama Proj ect

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    Pascua-Lama Proj ectPascua-Lama Proj ect

    Act ivit ies underw ayReceived Board of Direct or approval for development in

    July 2004

    Aw aiting environment al approvals

    Finalizing f iscal and t axat ion mat t ers

    I mplement ing Protocol regime

    Developing sustainable development communi t y programs

    Expect t o receive approvals and f inalize other f iscal and

    taxation mat t ers in lat e 2005

    Expect t o begin t hree-year const ruct ion schedule in 2006

    Product ion ant icipated for 2009

    Const ruct ion cost est imate approx imat ely

    $1.4-$1.5 bil l ion

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    P E R U

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    ALTO CHI CAMA PROJECTALTO CHI CAMA PROJECT

    LAS LAGUNAS NORTELAS LAGUNAS NORTE

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    LIMA

    Trujillo

    Pacific Ocean

    Cajamarca

    Arequipa

    Huamachuco

    HuarazPierina

    Alt o Chicama

    areaenlarged

    Yanacocha

    LOCATI ON

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    N0 25 50

    N0 25 50

    Mioc

    eneH

    SbeltN

    .Peru

    Mioc

    eneH

    SbeltN

    .Peru

    YanacochaYanacocha

    Alto ChicamaAlto Chicama

    PierinaPierina

    Trujillo

    Cajamarca

    Huamachuco

    HuarazPierina

    Alt o Chicama

    Yanacocha

    NYanacocha

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    P E R U

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    N0 25 50

    Glacier

    Yanacocha

    Lakes

    Quaternary undiff

    Neogene intrusives

    Paleogene -Neogene molasses

    Paleogene-Neogene intrusives

    Paleogene-Neogene volcanics

    U-Cretaceous-Paleogene molasses

    U-Cretaceous marine carbonates

    U-Cretaceous marine siliciclasticsL-Cretaceous intrusives

    L-Cretaceous marine carbonates

    L-Cretaceous marine siliciclastics

    Cretaceous-Paleogene intrusives

    Cretaceous marine volcanics

    Triassic-Jurassic marine limestones

    Triassic-Jurassic continental siliciclastics

    Triassic-Jurassic m arine siliciclastics

    Precambrian and Paleozoic basement

    Precam br i an andPaleozo ic Basem ent

    CretaceousSed imen t s

    Ter t i a ryVolcanics

    Cord i l le ra

    BlancaBa t ho l i t h

    Coastal

    Batholith

    Pier ina

    Al to Ch icam a

    REGI ONAL GEOLOGY

    NYanacocha

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    N0 25 50

    N or t he rn Pe ru

    W ell k n ow n go l d be lt

    Cenozo ic > 80 Moz > 6 0 M oz HS

    > 23 Moz Au-Cup o r p h y r y

    Paleozo ic > 6Moz

    Pat az d is t r i c t

    Pier ina

    Al to Ch icam aAl to Ch icam a

    Yanacocha

    REGI ONAL GOLD ENDOW MENT

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    DISTRICT GEOLOGY

    Calipuy FmInca FmFarrat FmCarhuaz Fm

    Chimu FmChicama Fm

    MINERALIZATION TYPE

    Epithermal Veins

    High Sulfidation

    Low Sulfidation

    Polymetallic

    Las LagunasNorte

    9.1 Moz Au

    DI STRI CT GEOLOGY

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F l o w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F i n e L a m i n a t e d A s h T u f f s

    F i n e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f f a c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i n e Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Miocene

    U n c o n f o r m i t y

    LLN GEOLOGY

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F lo w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F in e L a m i n a t e d A s h T u f f s

    F in e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f fa c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i ne Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Mioce

    ne

    U n c o n f o r m i t y

    LLN GEOLOGY

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    P E R U

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F l o w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F in e L a m i n a t e d A s h T u f f s

    F in e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f fa c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i ne Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Mioce

    ne

    U n c o n f o r m i t y

    LLN GEOLOGY

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    P E R U

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F lo w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F in e L a m i n a t e d A s h T u f f s

    F in e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f fa c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i ne Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Mioce

    ne

    U n c o n f o r m i t y

    LLN GEOLOGY

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F lo w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F in e L a m i n a t e d A s h T u f f s

    F in e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f fa c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i ne Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Mioce

    ne

    U n c o n f o r m i t y

    LLN GEOLOGY

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    P E R U

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    C o a l

    O v e r b u r d e nL a t e A n d e s i t i c T u f f a n d F lo w sL a t e A n d e s i t i c d o m e

    S h u l c a h u a n g a F l o w s

    S h u l c a h u a n g a D o m eE a r l y A n d e s i t i c F l o w s

    E a r l y A n d e s i t i c D o m eA n d e s i t i c T u f f B r e c c i a J u v e n i l e F ra g sA n d e s i t i c T u f f B r e c c i a

    F in e L a m i n a t e d A s h T u f f s

    F in e L a m i n a t e d C r y s t a l T u f f s

    D a c i t i c T u f f

    P o ly m i c t i c B r e c c i a T u f fa c e o u s M x

    Q F P T u f f a n d F l o w sQ F P D o m e

    F i ne Q t z P h y r i c A s h T u f f s

    M o n o m i c t i c B r e c c i a T u f fa c e o u s M x

    Q u a r t z S a n d s t o n e s

    M u d s t o n eC a r b o n a c e o u s M u d s t o n e

    C h i c a m a

    Upper

    Jurassic

    Lower

    Cretaceous

    Mioce

    ne

    U n c o n f o r m i t y

    LLN GEOLOGY

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    PROEXPLO 2005

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    Above : Si l ica r ep lacem ent i n m uds ton es and s i l t st ones

    Be low : Vugg y si l ica in t u f f u n i t s

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    MI NERALI ZATI ON

    OxideZo

    ne

    4000m

    Sulfid

    eZone

    Mixed

    Zone

    500 - 1000250 - 500

    125 - 25075 - 12550 - 7525 - 50

    Grade Thickness Au (g/t x m)

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    3700NW

    4200NW

    5200NW

    SECTI ONS

    4700NW

    N

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    Above left: Oxide matrix breccia Above right: Leached sandstone

    Below left: Sulfide remnant Below right: Coarse sulfide in breccia

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    RESERVE GROW TH

    0

    1

    2

    3

    4

    5

    6

    7

    8

    9

    1 0

    Q 1 - 2 0 0 1 Q 2 - 2 0 0 2 YE- 2 0 0 2 YE- 2 0 0 3 YE- 2 0 0 4

    Contained

    Ounces

    (Moz)

    Discovery drill hole

    Initial ResourceEstimate

    Initial ReserveEstimate

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    P E R U

    PROEXPLO 2005May 24-27, LimaCONSTRUCTION CAMP (XI/2004)

    CACTUS AND ORCHIDSCACTUS AND ORCHIDS

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    TRANSPLANTTRANSPLANT

    Alto Chicama Environment ProtectionAlto Chicama Environment Protection

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    P E R U

    PROEXPLO 2005May 24-27, LimaFORESTRY NURSERIESFORESTRY NURSERIES

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    P E R U

    PROEXPLO 2005May 24-27, LimaTHE TOP SOIL STRIPPINGTHE TOP SOIL STRIPPING

    AND TRANSFER CONTROLAND TRANSFER CONTROL

    Lagunas Nort e Proj ectLagunas Norte Proj ect

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    Locat ed in nort h-cent ral Peru, about 175 k ilometersfrom the Pierina Mine

    Oxide mineralizat ion sim ilar t o Pierina, w it h high-

    grade gold sur face out croppings and good metallurgy

    Open-pit , valley-f i l l crushing/ leaching operat ion

    Lagunas Nort e discovery announced on Apr il 23, 2002Proven and probable gold reserves of 9.1 m ill ion

    ounces

    1,350 square k ilomet er land posit ion w it h goodexplorat ion potent ial w it hin a 15 kilometer radius of

    Lagunas Nort e

    Lagunas Nort e Proj ectLagunas Norte Proj ect

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    P E R U

    PROEXPLO 2005May 24-27, Lima

    Act ivit ies underw ay

    The mine is mechanically complete

    Commissioning of equipm ent & facilit ies start ed in early Apri l

    2005

    Over 400,000 t ons of material placed on t he leach pad

    Manpower is 100% in place

    Product ion expected to commence in m id-June 2005

    Const ruct ion cost est imat e approx imat ely $340 mill ion

    Gold product ion is expect ed t o average approximat ely

    800,000 ounces per year at an average t otal cash costof about $155 per ounce for t he f irst t hree years

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    P E R U

    PROEXPLO 2005May 24-27, Lima